The Cenozoic history of the retreating Hellenic subduction system in the eastern
Mediterranean involves subduction, accretion, arc magmatism, exhumation, normal faulting …

Greece hosts a variety of magmatic-hydrothermal ore deposits/prospects with porphyry-and
epithermal styles playing a major role in its total gold endowment. These deposit types are …

The complexity of the plate interactions and associated crustal deformation in the Eastern
Mediterranean region is reflected in many destructive earthquakes that have occurred …

Mylonitic gneisses of the Bulgarian and Greek Rhodope were deformed under amphibolite-
facies conditions of medium pressure type metamorphism. The kinematic information …

Abstract The Cenozoic metallogeny in Greece includes numerous major and minor
hydrothermal mineral deposits, associated with the closure of the Western Tethyan Ocean …

The Serbo-Macedonian Massif is a basement complex in the Internal Hellenides of northern
Greece, situated between the Vardar Zone to the west and the Rhodope Massif to the east …

Some orogenic sedimentary basins are difficult to assign to a particular category. An
example is the hydrocarbon‐bearing Thrace Basin in the northern Aegean. It has more than …

The Aegean region experienced back-are extension related to the Hellenic subduction
system at least from the latest Oligocene to the present. We document Tertiary extension …

New low-temperature thermochronological data have been used to quantify the protracted,
Eocene–Miocene cooling histories of upper and lower plate rocks of the Kesebir–Kardamos …

The southern part of the Strandja Massif, northern Thrace, Turkey, comprises a basement of
various gneisses, micaschists and rare amphibolite, and a cover of metaconglomerate and …